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    Turbulence Approximation for Inhomogeneous Flows: Part II. The Numerical Simulation of a Penetrative Convection Experiment

    Source: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 003::page 482
    Author:
    André, J. C.
    ,
    De Moor, G.
    ,
    Lacarrère, P.
    ,
    Du Vachat, R.
    DOI: 10.1175/1520-0469(1976)033<0482:TAFIFP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The quasi-normal theory modified by the clipping approximation is used to construct a numerical model of vertically inhomogeneous turbulence in a Boussinesq fluid. The pressure-correlation terms are expressed according to recently proposed formulations. With the aid of the horizontal homogeneity assumption the model is applied to the description of a laboratory experiment on penetrative convection and the numerical results are compared to the experimental data. It is found that the model does reproduce the measured vertical variations of mean temperature, turbulent beat flux, eddy kinetic energy and temperature variance, as well as a third-order correlation such as the vertical flux of eddy kinetic energy. The stationarity of the vertical profiles of various turbulent quantities, when scaled by the convective velocity and temperature, is also verified.
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      Turbulence Approximation for Inhomogeneous Flows: Part II. The Numerical Simulation of a Penetrative Convection Experiment

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4152866
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    contributor authorAndré, J. C.
    contributor authorDe Moor, G.
    contributor authorLacarrère, P.
    contributor authorDu Vachat, R.
    date accessioned2017-06-09T14:18:44Z
    date available2017-06-09T14:18:44Z
    date copyright1976/03/01
    date issued1976
    identifier issn0022-4928
    identifier otherams-17018.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152866
    description abstractThe quasi-normal theory modified by the clipping approximation is used to construct a numerical model of vertically inhomogeneous turbulence in a Boussinesq fluid. The pressure-correlation terms are expressed according to recently proposed formulations. With the aid of the horizontal homogeneity assumption the model is applied to the description of a laboratory experiment on penetrative convection and the numerical results are compared to the experimental data. It is found that the model does reproduce the measured vertical variations of mean temperature, turbulent beat flux, eddy kinetic energy and temperature variance, as well as a third-order correlation such as the vertical flux of eddy kinetic energy. The stationarity of the vertical profiles of various turbulent quantities, when scaled by the convective velocity and temperature, is also verified.
    publisherAmerican Meteorological Society
    titleTurbulence Approximation for Inhomogeneous Flows: Part II. The Numerical Simulation of a Penetrative Convection Experiment
    typeJournal Paper
    journal volume33
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1976)033<0482:TAFIFP>2.0.CO;2
    journal fristpage482
    journal lastpage491
    treeJournal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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